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- The eastern China Continent has entered into the stage of rifting continental margin since Oligocene. 自漸新世，中國東部大陸進入了張裂的大陸邊緣階段。
- They were continental rift and passive continental margin basins formed as a result of the break-up of Gondwana and the spreading of Atlantic Ocean. 西非海岸盆地群的形成和發育,與中生代以來大西洋裂開和後期的持續擴張作用有關,是岡瓦納大陸解體和大西洋擴張形成的大陸裂谷和被動陸緣盆地。
- Volcanic rocks in Nadigangri formation could be nothing to do with plate subduction,but it was formed in extensional environment near continental margin which might be similar to rift. 那底崗日組火山岩應是與板塊消減作用無關的,類似於拉張環境的靠近大陸邊緣的類似於裂谷的環境中。
- Volcanic rifted margins are a kind of continental margin formed during continental breakup.Their geodynamic evolution is as complex as that of active margins. 摘要火山型被動陸緣是大陸解體過程中形成的一類陸緣類型，其演化過程與活動陸緣一樣複雜多變。
- The data and graphs from petrochemistry and geochemistry approve that the tectonic setting is continental margin arc. 岩石化學及地球化學的各種參數和圖解表明,其形成於陸緣島弧環境。
- The Lishui Jiaojiang Sag was a faulted basin developing on the continental margin from the late cretaceous epoch. 麗水、椒江凹陷是晚白堊世以來發展起來的大陸邊緣裂陷盆地。
- Tile study shows that the vocaniclastic turbidite deposited in a passive continental margin. 該區的火山碎屑濁積岩形成於被動大陸邊緣構造環境。
- The source roc k co uld be formed in the condition of relatively stable continental margin epicontin ental marine in micro-plate. 原岩形成於相對穩定的大陸邊緣-微板塊內的陸表海環境。
- The Xiaorequanzi copper (zinc) deposit is situated in the south of a paleovolcanic domain in Haerlik-Danahu late Palaeozoic continental margin island. 摘要位於東天山的小熱泉子銅（鋅）礦床是該地區有較大開發意義的礦床類型。
- The study on gas hydrate enrichment in the passive continental margin showed the importance of thermogenic gas for forming gas hydrate. 對被動大陸邊緣水合物的富集規律研究表明：熱解成因天然氣水合物在被動大陸邊緣佔有重要地位，被動陸緣的活動斷裂、底辟構造、滑塌堆積、斷裂坡折帶和海底扇砂體對天然氣水合物的富集過程具有重要的控制作用。
- General features of ocean. Movement of ocean: wave, tides and ocean current. Eros ional and depositional coast. Continental margin and ocean basin. 海洋的一般特徵。海洋的運動：波浪、洋流和潮汐。侵蝕型海岸和沉積型海岸。大陸邊緣和洋盆。
- Teng, Louis S.(1992) Geotectonic evolution of Tertiary continental margin basins of Taiwan. Petroleum Geology of Taiwan, 27, 1-19. 鄧屬予(1992)台灣第三紀陸緣盆地的地體演化。台灣石油地質，第27號，第1-19頁。
- Gong Zhasheng and Li Sitian. Basin Analysis and Petroleum Accumulation of the Northern South China Sea Continental Margin Basin. Beijing: Science Press, 1997. 龔再升,李思田。南海北部大陸邊緣盆地分析與油氣聚集。北京:科學出版社,1997。
- In very wide basins the down-drag of the enormous cooling floor dominates processes at the continental margin and produces the deceptive similarities to half-grabens. 在十分廣闊的盆地中，大陸邊緣主要過程是受巨大冷卻板塊的向下拖曳，併產生類似半地塹的假象。
- This is apparently related to the tectonic setting of Shandong,namely, the continental margin where the Pacific Plate collided against the Eurasian Plate. 之所以如此,顯然與山東所處的大地構造位置,即太平洋板塊與歐亞板塊相互碰撞的陸緣地帶密切相關。
- Bayinbuluke formation was been mostly distributed in Lanati of western tianshan, The tectonic location at the Paleozoic active continental margin of southern Yili basin. 摘要巴音布魯克組主要分佈於新疆西天山那拉提一帶，構造上位於伊犁盆地南緣活動帶，岩性主要為一套糜棱岩化、碎裂岩化中基性火山岩、正常沉積碎屑岩夾灰岩。
- The south eastern margin of the Pan Cathaysian continental group consists of the Yangtze continental plate and the paleo continental margin of South China. 泛華夏大陸群東南緣多島弧盆系統從東南向西北由浙閩-雲開島弧、閩粵弧后盆地、武夷山島弧、湘桂弧后盆地、江南島弧、雪峰山前陸隆起等幾部分組成。
- The coarse sediments have generally accumulated along the continental margins. 粗粒沉積物一般沿大陸邊緣堆積。
- Otherwise with Paleotethys closing in late Triassic period,the pull-apart continental margin reversed in Indo-China movement creating Indo-Chinafolded orogeny. 晚三疊紀隨古特提斯的閉合,經印支運動張裂陸緣發生反轉,形成印支褶皺造山帶。
- Lantanbulake Formation of Changcheng System is composed of meta-volcanics and volcaniclastics which belong to island arc or active continental margin deposits. 長城系亂灘布拉克組由一套變火山岩、火山碎屑岩組成，屬島弧或活動陸緣沉積；
